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High-temperature X-ray diffraction study of uranium-neptunium mixed oxides

机译:铀n混合氧化物的高温X射线衍射研究

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Incorporating minor actinides (MAs = Am, Np, Cm) in UO_2 fertile blankets is a viable option to recycle them. Despite this applied interest, phase equilibria between uranium and MAs still need to be thoroughly investigated, especially at elevated temperatures. In particular, few reports on the U-Np-O system are available. In the present work, we provide for the first time in situ high-temperature X-ray diffraction results obtained during the oxidation of (U_(1-y)Np_y)O_2 uranium-neptunium mixed oxides up to 1373 K and discuss subsequent phase transformations. We show that (i) neptunium stabilizes the UO_2-type fluorite structure at high temperature and that (ii) the U_3O_8-type orthorhombic structure is observed in a wide range of compositions. We clearly demonstrate the incorporation of neptunium in this phase, which was a controversial question in previous studies up to now. We believe it is the particular stability of the tetravalent state of neptunium that is responsible for the observed phase relationships.
机译:将微量act系元素(MAs = Am,Np,Cm)掺入UO_2肥沃的毯子中是回收它们的可行选择。尽管有这种应用兴趣,但仍需彻底研究铀与MA的相平衡,特别是在高温下。特别是,关于U-Np-O系统的报告很少。在本工作中,我们首次提供了在氧化过程中(U_(1-y)Np_y)O_2铀-mixed混合氧化物氧化至1373 K的高温X射线衍射结果,并讨论了随后的相变。我们表明(i)ept在高温下稳定了UO_2型萤石结构,并且(ii)在广泛的组成范围内观察到U_3O_8型正交晶结构。我们清楚地证明了在这一阶段掺入n,这是迄今为止迄今为止研究中一个有争议的问题。我们认为,observed的四价态的特殊稳定性决定了所观察到的相位关系。

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